Carbon dioxide activation and alkali compound formation. I. Vibrational characterization of oxalate intermediates

The activation of CO₂ in thin potassium layers adsorbed on Cu(1 1 1) has been studied with time-evolved Fourier transform-infrared reflection absorption spectroscopy. The growth of thin layers by reactive evaporation of potassium in a CO₂ atmosphere permits control of the K:CO₂ stoichiometry, which strongly affects the selectivity in the formation of intermediates and the decomposition pathways of the layer. Layers grown in a CO₂ rich atmosphere exhibit the preferential growth of stoichiometric potassium oxalate K₂C₂O₄ (D_2h). The molecular identity of oxalate with D_2h symmetry is confirmed by vibrational spectra utilizing isotopic substitution methods (¹³CO₂ and C¹⁸O₂) and by the use of isotopic mixtures of CO₂/C¹⁸O₂ and CO₂/¹³CO₂. A comparison of the isotope data with theoretical calculations gives an estimated OCO bond angle in oxalate of 132°. Far-IR spectra obtained with synchrotron radiation indicate the equivalent interaction of all oxygen atoms with the potassium. A comparison of the vibrational data with theoretical ab initio calculations confirms the structural model of an oxalate species that is bulk coordinated with no strong directional bonding and all oxygen atoms equally interacting with potassium.At medium and low CO₂:K ratios, very complex vibrational spectra are observed, indicating the formation of an oxalate surface species with C_2v symmetry in addition to D_2h⁻ oxalate, CO₂⁻ and CO₂²⁻ species.